Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Clinopyroxene Subgroup from
Uglvik peridotite body, Uglvik, Otrøya, Midsund, Molde, Møre og Romsdal, Norway


Locality type:Outcrop
Classification
Species:'Clinopyroxene Subgroup' (not an IMA approved species)
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Clinopyroxene Subgroup data
Locality Data:Click here to view Uglvik peridotite body, Uglvik, Otrøya, Midsund, Molde, Møre og Romsdal, Norway
Data Identifiers
Mindat Occurrence Record ID:646557
Long-form Identifier:1:3:646557:5
GUID (UUID V4):0
Nearest other occurrences of Clinopyroxene Subgroup
2.2km (1.4 miles) ⓘMagerøy Eclogite, Korveneset, Otrøya, Midsund, Molde, Møre og Romsdal, Norway
18.9km (11.7 miles) ⓘBardane, Fjørtofta, Haram, Ålesund, Møre og Romsdal, Norway
27.5km (17.1 miles) ⓘHaramsneset, Haramsøya, Haram, Ålesund, Møre og Romsdal, Norway
41.1km (25.6 miles) ⓘFestøya, Ørsta, Møre og Romsdal, Norway
64.7km (40.2 miles) ⓘHamarsneset Beach, Runde Island, Sørøyane, Herøy, Møre og Romsdal, Norway
77.8km (48.3 miles) ⓘSandvik peridotite, Gurskøya, Sande, Møre og Romsdal, Norway
80.0km (49.7 miles) ⓘVestbrona Formation, Kristiansund, Møre og Romsdal, Norway
94.5km (58.7 miles) ⓘEikremsæterfoss eclogite, Almklovdalen, Vanylven, Møre og Romsdal, Norway
95.1km (59.1 miles) ⓘAlmklovdalen, Vanylven, Møre og Romsdal, Norway
95.8km (59.5 miles) ⓘSandviknes, Årsheim, Selje, Stad, Vestland, Norway
References
Van Roermund, H.L.M et al. (2000): Super-silicic garnet microstructures from an orogenic garnet peridotite, evidence for an ultradeep (>6GPa) origin. Journal of Metamorphic Geology 18: 135-147
 
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